The vegetation pattern of siliceous boulder snow beds (Dicranoweision crispulae all. nov. prov.) of Svalbard was investigated by using transect studies in several places on Spitsbergen. Dicranoweisia crispula is the best diagnostic species. It is found throughout the whole snow bed, is a good differential species against Racomitrium lanuginosum communities above the snow bed, and does not occur on basic rocks. Three Andreaea spp. are also among the most important members of these communities. They are all acidophilous, but with different pH preferences. Eight weakly acidophilous species lacking both on basic and on gneissic/granitic rocks, are reported from Svalbard. Half of these are characteristic species of Dicranoweision crispulae on Sv...
The relationship between plant occurrence and moraine surface conditions was studied in three areas ...
The relationship between plant occurrence and moraine surface conditions was studied in three areas ...
The relationship between distribution of bryophytes and soil conditions on deglaciated arctic terrai...
Abstract: The relationship between distribution of bryophytes and soil conditions on deglaciated arc...
In this work, the authors estimate the species abundance and the characteristics of ground cover (he...
The main gradient in vascular plant, bryophyte and lichen species composition in alpine areas, struc...
The development of vegetation in Arctic glacier forelands has been described as unidirectional, non-...
The development of vegetation in Arctic glacier forelands has been described as unidirectional, non-...
The development of vegetation in Arctic glacier forelands has been described as unidirectional, non-...
The development of vegetation in Arctic glacier forelands has been described as unidirectional, non-...
Mosses are an impotent component of developing plant communities of glacier forelands of the Russian...
The main gradient in vascular plant, bryophyte and lichen species composition in alpine areas, struc...
Mosses are an impotent component of developing plant communities of glacier forelands of the Russian...
Aim: Pleistocene erratic boulders are rocks that were relocated by glaciers during the Ice Ages. Whe...
The Ninth Symposium on Polar Science/Ordinary sessions: [OB] Polar biology, Wed. 5 Dec. / Entrance H...
The relationship between plant occurrence and moraine surface conditions was studied in three areas ...
The relationship between plant occurrence and moraine surface conditions was studied in three areas ...
The relationship between distribution of bryophytes and soil conditions on deglaciated arctic terrai...
Abstract: The relationship between distribution of bryophytes and soil conditions on deglaciated arc...
In this work, the authors estimate the species abundance and the characteristics of ground cover (he...
The main gradient in vascular plant, bryophyte and lichen species composition in alpine areas, struc...
The development of vegetation in Arctic glacier forelands has been described as unidirectional, non-...
The development of vegetation in Arctic glacier forelands has been described as unidirectional, non-...
The development of vegetation in Arctic glacier forelands has been described as unidirectional, non-...
The development of vegetation in Arctic glacier forelands has been described as unidirectional, non-...
Mosses are an impotent component of developing plant communities of glacier forelands of the Russian...
The main gradient in vascular plant, bryophyte and lichen species composition in alpine areas, struc...
Mosses are an impotent component of developing plant communities of glacier forelands of the Russian...
Aim: Pleistocene erratic boulders are rocks that were relocated by glaciers during the Ice Ages. Whe...
The Ninth Symposium on Polar Science/Ordinary sessions: [OB] Polar biology, Wed. 5 Dec. / Entrance H...
The relationship between plant occurrence and moraine surface conditions was studied in three areas ...
The relationship between plant occurrence and moraine surface conditions was studied in three areas ...
The relationship between distribution of bryophytes and soil conditions on deglaciated arctic terrai...